Faulting

Faulting is a geological process where rocks along a crack or fracture, called a fault, move relative to each other. This movement can occur suddenly during an earthquake or gradually over time. Faults can cause the Earth's surface to shift, creating features like cliffs or valleys. Essentially, faulting is nature’s way of releasing built-up stress in the Earth's crust, often revealing evidence of past tectonic activity. It’s a key factor in shaping our planet’s landscape and understanding seismic risks.